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A Thermal Wave Approach for Heat Transfer in a Nonuniform Soil

Mostafa A. Karam

GenCorp Aerojet, 1100 W. Hollyvale St., Azusa, CA 91702 USA



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Fig. 1 Problem formulation

 


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Fig. 2 Logarithm of the magnitude of the frequency-dependent temperature amplitude -log|T(z,{omega})/T(0,{omega})| for a soil having thermal properties described by the increasing (labeled 1) and decreasing (labeled 2) exponential profiles of Eq. [26] (N = 50 sublayers)

 


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Fig. 3 Phase of the frequency-dependent temperature -{phi}(z,{omega}) for a soil having thermal properties described by the increasing (labeled 1) and decreasing (labeled 2) exponential profiles of Eq. [26] (N = 50 sublayers)

 


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Fig. 4 The logarithm of the first derivative of frequency-dependent temperature amplitude -log|T'(z,{omega})/T'(0,{omega}) for a soil having thermal properties described by the increasing (labeled 1) and decreasing (labeled 2) exponential profiles of Eq. [26] (N = 50 sublayers)

 


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Fig. 5 The phase difference |{phi}(z,{omega}) - {phi}d(z,{omega})| for a soil having thermal properties described by the increasing (labeled 1) and decreasing (labeled 2) exponential profiles of Eq. [26] (N = 50 sublayers)

 


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Fig. 6 The time-dependent temperature for a soil having thermal properties described by the increasing linear profile of Eq. [31]

 


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Fig. 7 The time-dependent temperature for a soil having thermal properties described by the decreasing linear profile of Eq. [31]

 





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The SCI Journals Agronomy Journal Crop Science
Journal of Natural Resources
and Life Sciences Education
Vadose Zone Journal
Journal of Plant Registrations Journal of
Environmental Quality
The Plant Genome
Copyright © 2000 by the Soil Science Society of America.